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北部フォッサ・マグナ地域の第三紀層にみられる堆積構造についての研究
http://hdl.handle.net/10091/4319
http://hdl.handle.net/10091/4319019d37c4-16ee-4831-b7be-a1c5a17c7478
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
Liberal_arts_S07-06.pdf (5.6 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||||||||
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| 公開日 | 2010-02-12 | |||||||||||||||
| タイトル | ||||||||||||||||
| タイトル | 北部フォッサ・マグナ地域の第三紀層にみられる堆積構造についての研究 | |||||||||||||||
| タイトル | ||||||||||||||||
| タイトル | Studies on the Sedimentary Structures Observed in the Tertiary Formation of the Northern Fossa Magna | |||||||||||||||
| 言語 | ||||||||||||||||
| 言語 | jpn | |||||||||||||||
| 資源タイプ | ||||||||||||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||||||||||||
| タイプ | departmental bulletin paper | |||||||||||||||
| 著者 |
田中, 邦雄
× 田中, 邦雄
× 寺平, 宏
× 遠藤, 忠慶
× 平出, 友伯
× 熊井, 深志
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| 出版者 | ||||||||||||||||
| 出版者 | 信州大学教養部 | |||||||||||||||
| 引用 | ||||||||||||||||
| 内容記述 | 信州大学教養部紀要. 第二部, 自然科学 7: 49-90(1973) | |||||||||||||||
| 書誌情報 |
信州大学教養部紀要. 第二部, 自然科学 巻 7, p. 49-90, 発行日 1973-03-15 |
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| 抄録 | ||||||||||||||||
| 内容記述 | 1. In the Tertiary Formation of the Northern Fossa Magna many Sedimentary structures are observed. Judging from the ongms, they are divided into following; 1. the gravitational loading (Load casts, Convolute bedding), 2. the turvidity currents (Flute casts, Groove casts), 3. the bottom .cllrrents (Ripple mark, Crescent casts), 4. the injection (Clastic dike), 5. the subaqueous slide (Slump structure, Rubble bedding, Norimaki structure, Bent chunks). We investigated them in detai1. 2. The Sedimentary structures are essentially different from the Geological structures by the tectonic movement, but in this area they are closely connected with the Geological structures, for instance, Saigawa Fractured Zone runs along the west side of the Central Uplift Zone and Nakatsllchi Fractured Zone along the south side of Otari Uplift Zone. The sedimentary structures of these Fractured Zones told that two Uplift Zone made the uplift movement with the deposite of sedimentary rocks. 3. That area rich in sedimentarystructures along the south side of Otari Uplift Zone was called by Teruo HIRABAYASHI Nakatsuchi Crushered Zone, but we adovocate to name it Nakatsuchi Fractured Zone. | |||||||||||||||
| 資源タイプ（コンテンツの種類） | ||||||||||||||||
| ISSN | ||||||||||||||||
| 収録物識別子タイプ | ISSN | |||||||||||||||
| 収録物識別子 | 0583-0613 | |||||||||||||||
| 書誌レコードID | ||||||||||||||||
| 収録物識別子タイプ | NCID | |||||||||||||||
| 収録物識別子 | AN0012116X | |||||||||||||||
| 出版タイプ | ||||||||||||||||
| 出版タイプ | VoR | |||||||||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||||||
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Cite as
田中, 邦雄, 寺平, 宏, 遠藤, 忠慶, 平出, 友伯, 熊井, 深志, 1973, 北部フォッサ・マグナ地域の第三紀層にみられる堆積構造についての研究: 信州大学教養部, 49–90 p.
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